does δ18o of o2 record meridional shifts in tropical rainfall?
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2017
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Abstract
Marine sediments, speleothems, paleo-lake elevations, and ice core
methane and δ18O of O2
(δ18Oatm) records provide ample evidence
for repeated abrupt meridional shifts in tropical rainfall belts
throughout the last glacial cycle. To improve understanding of the
impact of abrupt events on the global terrestrial biosphere, we
present composite records of δ18Oatm and
inferred changes in fractionation by the global terrestrial
biosphere (ΔεLAND) from discrete gas
measurements in the WAIS Divide (WD) and Siple Dome (SD) Antarctic
ice cores. On the common WD timescale, it is evident that maxima in
ΔεLAND are synchronous with or shortly
follow small-amplitude WD CH4 peaks that occur within
Heinrich stadials 1, 2, 4, and 5 – periods of low atmospheric
CH4 concentrations. These local CH4 maxima have been
suggested as markers of abrupt climate responses to Heinrich
events. Based on our analysis of the modern seasonal cycle of gross
primary productivity (GPP)-weighted δ18O of
terrestrial precipitation (the source water for atmospheric
O2 production), we propose a simple mechanism by which
ΔεLAND tracks the centroid latitude of
terrestrial oxygen production. As intense rainfall and oxygen
production migrate northward, ΔεLAND
should decrease due to the underlying meridional gradient in
rainfall δ18O. A southward shift should increase
ΔεLAND. Monsoon intensity also
influences δ18O of precipitation, and although we
cannot determine the relative contributions of the two mechanisms,
both act in the same direction. Therefore, we suggest that abrupt
increases in ΔεLAND unambiguously imply
a southward shift of tropical rainfall. The exact magnitude of this
shift, however, remains under-constrained by ΔεLAND.
| Reference Key |
seltzer2017climatedoes
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|---|---|
| Authors | ;A. M. Seltzer;C. Buizert;D. Baggenstos;E. J. Brook;J. Ahn;J.-W. Yang;J. P. Severinghaus |
| Journal | proceedings - 16th ieee/acis international conference on computer and information science, icis 2017 |
| Year | 2017 |
| DOI |
10.5194/cp-13-1323-2017
|
| URL | |
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